FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2771204274> ?p ?o ?g. }

• W2771204274 abstract "The Northern Forest is a complex, heterogeneous environment which is undergoing changes in response to anthropogenic forcing factors. It is, therefore, necessary to quantify how trees have responded to environmental conditions in the past and may respond in the future. Traditional tree-ring width analysis enables the creation of temporally-expansive, annually-resolved records of yearly variability in tree growth. These tree-ring archives are well suited for researching which climate drivers have impacted forest growth most significantly and for identifying changes in the temporal stability of the climate signal over the 20th and 21st century. To perform this analysis, tree-ring width chronologies were developed for an eastern hemlock (Tsuga canadensis) stand, located at the Abbey Pond site in East Middlebury, Vermont, and red spruce (Picea rubens) stand, located in the Cape National Research Area (NRA) site, near Goshen Four Corners, Vermont, using increment cores sampled in 2010. A subset of each chronology was analyzed using blue intensity analysis (BIA), a novel dendrochronological technique which has been developed as a proxy for maximum latewood density (MXD) analysis. MXD has been utilized extensively in summer temperature reconstructions as it is capable of capturing a stronger, summer temperature signal. This study represents the first attempt to use BIA with eastern hemlock and red spruce trees and the first study within the US Northeast to incorporate BIA into dendroclimatological analysis. A combination of temperature, precipitation, and novel climate datasets were assembled to explore the drivers of growth of each forest stand. Several climate datasets, namely total percent cloudiness, total percent possible sunshine, and sunshine hours, to the best of our knowledge, have not been incorporated into past dendrochronology studies conducted in Vermont or the Northeastern US. Linear mixed model analysis was used to determine how much variability in annual growth could be attributed to climate drivers. 34% of the variance (R2 = 0.34) in the Abbey Pond TRW chronology was accounted for using summer (JJA) precipitation and June PDSI as predictors of growth. 35% of the variance in the Abbey Pond BIA chronology was accounted for using minimum September temperatures and total percent cloudiness (TPC). Previous year temperatures in July and August and present year minimum temperatures in September accounted for 33% of the annual variance in the Cape NRA TRW chronology. Minimum spring temperatures were only able to account for 6.8% of the annual variance in the Cape BIA chronology." @default.
• W2771204274 created "2017-12-22" @default.
• W2771204274 creator A5082663613 @default.
• W2771204274 date "2016-01-01" @default.
• W2771204274 modified "2023-09-27" @default.
• W2771204274 title "NEW DENDROCHRONOLOGICAL APPROACHES TO IDENTIFYING CLIMATE DRIVERS IN NORTHERN CONIFERS" @default.
• W2771204274 cites W1515936669 @default.
• W2771204274 cites W154286391 @default.
• W2771204274 cites W1561012136 @default.
• W2771204274 cites W1879909559 @default.
• W2771204274 cites W1971696237 @default.
• W2771204274 cites W1973255192 @default.
• W2771204274 cites W1981187949 @default.
• W2771204274 cites W1985201273 @default.
• W2771204274 cites W1988990937 @default.
• W2771204274 cites W2004683157 @default.
• W2771204274 cites W2005240403 @default.
• W2771204274 cites W2012179371 @default.
• W2771204274 cites W2013183371 @default.
• W2771204274 cites W2018927543 @default.
• W2771204274 cites W2019088561 @default.
• W2771204274 cites W2020070933 @default.
• W2771204274 cites W2022332001 @default.
• W2771204274 cites W2025114417 @default.
• W2771204274 cites W2029970974 @default.
• W2771204274 cites W2034229104 @default.
• W2771204274 cites W2039261637 @default.
• W2771204274 cites W2042954571 @default.
• W2771204274 cites W2043826548 @default.
• W2771204274 cites W2047627323 @default.
• W2771204274 cites W2053644856 @default.
• W2771204274 cites W2061761642 @default.
• W2771204274 cites W2070330841 @default.
• W2771204274 cites W2070655959 @default.
• W2771204274 cites W2084052267 @default.
• W2771204274 cites W2087787921 @default.
• W2771204274 cites W2092312352 @default.
• W2771204274 cites W2094666965 @default.
• W2771204274 cites W2103303955 @default.
• W2771204274 cites W2108817398 @default.
• W2771204274 cites W2110708328 @default.
• W2771204274 cites W2115476971 @default.
• W2771204274 cites W2121013971 @default.
• W2771204274 cites W2126473499 @default.
• W2771204274 cites W2140266995 @default.
• W2771204274 cites W2145327055 @default.
• W2771204274 cites W2145497169 @default.
• W2771204274 cites W2146664101 @default.
• W2771204274 cites W2148119123 @default.
• W2771204274 cites W2154504186 @default.
• W2771204274 cites W2159252479 @default.
• W2771204274 cites W2163997486 @default.
• W2771204274 cites W2165562007 @default.
• W2771204274 cites W2168115048 @default.
• W2771204274 cites W2171578526 @default.
• W2771204274 cites W2172478360 @default.
• W2771204274 cites W2229711034 @default.
• W2771204274 cites W2242973286 @default.
• W2771204274 cites W2320965205 @default.
• W2771204274 cites W2594864454 @default.
• W2771204274 cites W2798159342 @default.
• W2771204274 cites W2802978358 @default.
• W2771204274 cites W3021510377 @default.
• W2771204274 cites W3188190260 @default.
• W2771204274 cites W807364279 @default.
• W2771204274 hasPublicationYear "2016" @default.
• W2771204274 type Work @default.
• W2771204274 sameAs 2771204274 @default.
• W2771204274 citedByCount "0" @default.
• W2771204274 crossrefType "journal-article" @default.
• W2771204274 hasAuthorship W2771204274A5082663613 @default.
• W2771204274 hasConcept C100970517 @default.
• W2771204274 hasConcept C107054158 @default.
• W2771204274 hasConcept C119857082 @default.
• W2771204274 hasConcept C127313418 @default.
• W2771204274 hasConcept C132651083 @default.
• W2771204274 hasConcept C153294291 @default.
• W2771204274 hasConcept C159985019 @default.
• W2771204274 hasConcept C166957645 @default.
• W2771204274 hasConcept C181536285 @default.
• W2771204274 hasConcept C18678713 @default.
• W2771204274 hasConcept C18903297 @default.
• W2771204274 hasConcept C192562407 @default.
• W2771204274 hasConcept C197115733 @default.
• W2771204274 hasConcept C205649164 @default.
• W2771204274 hasConcept C2779237806 @default.
• W2771204274 hasConcept C2780148112 @default.
• W2771204274 hasConcept C2780502288 @default.
• W2771204274 hasConcept C30407753 @default.
• W2771204274 hasConcept C39432304 @default.
• W2771204274 hasConcept C41008148 @default.
• W2771204274 hasConcept C49204034 @default.
• W2771204274 hasConcept C68753075 @default.
• W2771204274 hasConcept C86803240 @default.
• W2771204274 hasConceptScore W2771204274C100970517 @default.
• W2771204274 hasConceptScore W2771204274C107054158 @default.
• W2771204274 hasConceptScore W2771204274C119857082 @default.
• W2771204274 hasConceptScore W2771204274C127313418 @default.
• W2771204274 hasConceptScore W2771204274C132651083 @default.
• W2771204274 hasConceptScore W2771204274C153294291 @default.

• next